The following is a map unit description from the "Soil
Survey of Barnstable County, Massachusetts (Fletcher, 1993)"

HeB-Hinckley sandy loam, 3 to 8 percent slopes. This
very deep, gently sloping, excessively drained soil is in broad
hummocky areas and on low hills on outwash plains. It makes up
about 0.6 percent (1 @595 acres) of the survey area. It is mapped
mainly in the Enfield-Merrimac-Carver general soil map unit.
Areas are irregular in shape and range from 5 to 1,000 acres in
size.

Typically, the surface is covered with an organic layer. This
layer is about 2 inches of loose, undecomposed pine needles,
leaves, and twigs and 1 inch of partly decomposed and well
decomposed organic material. The surface layer is very friable
sandy loam about 2 inches thick. The upper 1 inch is black, and
the lower 1 inch is dark grayish brown. The subsoil is about 15
inches thick. The upper 1 inch is dark reddish brown, friable
gravelly sandy loam; the next 7 inches is yellowish brown,
friable gravelly sandy loam; and the lower 7 inches is yellowish
brown, friable gravelly loamy coarse sand. The substratum extends
to a depth of 65 inches or more. It is brownish yellow, loose
very gravelly coarse sand in the upper 37 inches and light
yellowish brown, loose gravelly coarse sand in the lower part.

Included with this soil in mapping are small areas of Carver,
Enfield, Merrimac, and Plymouth soils. Also included are areas
where slopes are less than 3 percent or more than 8 percent.
Included soils make up about 25 percent of this unit.

Permeability is rapid in the subsoil of the Hinckley soil and
very rapid in the substratum. Available water capacity is low.
Depth to the seasonal high water table is more than 6 feet.

Most areas are used as woodland. Some areas have been
developed for homesites, and a few areas are farmed.

This soil is poorly suited to cultivated crops. The low
available water capacity and the hazard of erosion are management
concerns. Irrigation is needed for most cultivated crops. Mixing
plant residue and manure into the surface layer increases the
available water capacity. Farming on the contour or across the
slope, terracing, stripcropping, including grasses and legumes in
the crop rotation, growing cover crops, and applying a system of
conservation tillage help to control runoff and erosion.

This soil is poorly suited to hay and pasture. The main
management objective is the prevention of overgrazing, which
reduces the hardiness and density of desirable plants. Proper
stocking rates, timely grazing, and restricted use during wet
periods help to maintain plant density and minimize surface
compaction.

Because of the droughtiness, this soil is poorly suited to
woodland. Thinning dense stands to standard stocking levels
results in more vigorous tree growth. Diseased, deformed, and
otherwise undesirable trees should be removed when the stands are
thinned. The most common trees are eastern pitch pine, white oak,
scarlet oak, black oak, and eastern white pine. Generally, these
trees are of poor quality.

This soil is suitable as a site for buildings with or without
basements. The droughtiness is a limitation affecting lawns and
shallow-rooted trees and shrubs. Adding a layer of topsoil and
frequently watering during dry periods help to overcome this
limitation. The soil readily absorbs but may not adequately
filter the effluent in septic tank absorption fields. The poor
filtering capacity may result in the pollution of ground water.
The hazard of pollution increases with the density of housing.
Precautionary measures may be necessary in some areas.